karstification 中文意思是什麼
karstification
解釋
喀斯特化-
Variation of mechanical property of marlite in process of karstification and weathering in three gorges region
三峽庫區泥灰質巖石溶蝕作用的微觀研究 -
The formation of carbonate reservior is controlled by the overlaid c - p strata and the intensity of karstification which was related to the palaeo geomorphy and palaeodrainage system
下古生界碳酸鹽巖裂縫溶蝕型儲集層的發育特徵以有無上古覆蓋是巖溶發育的前提；古地貌、古水系控制巖溶發育強度。 -
The paper takes an example of condensed gas feild in qianmiqiao buried - hills. based on the research of formation and development of the buried - hills, three important subjects in the research are discussed with the application of advanced technical and methods ( namely, balanced cross sections, analysis of carbon isotope, mensuration of reservoir fluid inclusion ) : ( 1 ) the development of karstification and characters of reservoir in ordovician ; ( 2 ) lower tertiary ( es3 ) source in the depression nearby ; ( 3 ) the hydrocarbon generation history, migration phase and reservoir formation history
論文以千米橋潛山凝析氣藏為例，在研究潛山形成演化基礎上，採用先進技術手段（平衡剖面技術、碳同位素分析、儲層流體包裹體測定） ，討論了該潛山油氣藏研究中三個重要問題： （ 1 ）古巖溶發育與奧陶系儲層特徵； （ 2 ）臨近凹陷下第三系油氣源： （ 3 ）油氣生成史與運移期次以及成藏歷史。 -
It was considered that karstification is the base of reservior formation, and lithology and faulting control the formation and development of internal reservior
其發育規律為：巖溶作用是下古生界儲集層發育的基礎；巖性和斷裂作用決定內幕儲層的形成與發育。 -
Based on the ground outcrops and drilling core samples, and two - dimensional seismic data in this paper, through a comprehensive evaluation and research of the reservoir characteristics, the authors clarifies that the dolomite of the upper sinian dengying formation and the grain limestone of the lower silurian shiniulan formation are main reservoir rocks in the research area, and the sedimentary facies, karstification, and the number of cracks are the main controlling factors of the reservoir quality
以地表露頭、鉆井資料及二維地震資料為基礎，通過儲層特徵綜合評價研究，認為上震旦統燈影組白雲巖、下志留統石牛欄組顆粒灰巖為區內的主要儲集巖，沉積相、巖溶作用及裂縫發育程度為儲層發育的主控因素。 -
This paper summarizes seven kinds of geological factors advantageous for karstification, such as the lithology, the strata framework, the geological strature, the paleo - relief, the paleo - climate, the former pore space system and the later reconstruction in embedding period
摘要分析了巖溶發育的7種地質因素，即巖性、地層結構、地質構造、佔地貌、古氣候、先存孔洞系統以及埋藏期的後期改造等。 -
Abstract : according to observation and study, the paleokarstifications of ordovician could be classified into 6 periods, i. e. depositional karstification, weathering curst karstification, burial karstification, semi - burial structural karstification, second burial karstification stage, its karstic types have mainly deposition karst, emergence karst, burial karst, wqueezing - water and structural karst or hot - water karst, and its karst - rocks can be distributed to two kinds of types, i. e. karst - sedimentary rock and karst - regenerated rock, and further to 8 subcategories and 5 sub - sub - categories in the north of anhui, china
文摘:研究表明，皖北奧陶系古巖溶可劃分為沉積巖溶作用期、風化殼巖溶作用期、埋藏巖溶作用期、構造巖溶作用期和二次埋藏巖溶作用期；其巖溶類型主要有沉積巖溶、風化殼巖溶、埋藏巖溶或壓釋水巖溶和構造巖溶或熱水巖溶四種類型；其巖溶巖包括巖溶沉積巖和巖溶改造巖兩個大類，並可進一步劃分出8個亞類和5個子亞類。 -
According to observation and study, the paleokarstifications of ordovician could be classified into 6 periods, i. e. depositional karstification, weathering curst karstification, burial karstification, semi - burial structural karstification, second burial karstification stage, its karstic types have mainly deposition karst, emergence karst, burial karst, wqueezing - water and structural karst or hot - water karst, and its karst - rocks can be distributed to two kinds of types, i. e. karst - sedimentary rock and karst - regenerated rock, and further to 8 subcategories and 5 sub - sub - categories in the north of anhui, china
研究表明，皖北奧陶系古巖溶可劃分為沉積巖溶作用期、風化殼巖溶作用期、埋藏巖溶作用期、構造巖溶作用期和二次埋藏巖溶作用期；其巖溶類型主要有沉積巖溶、風化殼巖溶、埋藏巖溶或壓釋水巖溶和構造巖溶或熱水巖溶四種類型；其巖溶巖包括巖溶沉積巖和巖溶改造巖兩個大類，並可進一步劃分出8個亞類和5個子亞類。 -
Huge deep fractures in the east of china have a little influence on the pore of carbonatite reservoir of ? - o stratum in the regions of zhuangxi and chengdao. the karstification which probably happened at xishan tectogenesis period is also very limited
我國東部深大斷裂對樁西、埋島地區寒武一奧陶系碳酸鹽巖的儲層孔隙影響很小，可能發生在喜山期的巖溶作用（深部流體帶來的巖溶作用）也是十分有限的。 -
3. it is discussed that the buried hill reservoir in this zone experienced karstification in caledonian - early hercynian, indosinian and mid yenshan movement period, and it is indicated that karst formed in late indosinian and mid yenshan movement period are the key periods to form fine reservoir
3探討了該區潛山儲層形成經歷加里東、海西早期、印支和燕山中期運動抬升型巖溶作用，指出印支、燕山中期運動抬升型巖溶是形成良好儲集層的關鍵。 -
Vertical zonation of karstification and its engineering geological significance
巖溶發育垂直分帶及其工程地質意義
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